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Sulphur isotopes in metamorphosed Precambrian Fe-Pb-Zn-Cu sulphides and baryte at Aggeneys and Gamsberg, South Africa

Published online by Cambridge University Press:  05 July 2018

K. von Gehlen ,
H. Nielsen ,
I. Chunnett  and
A. Rozendaal
K. von Gehlen
Affiliation:
Institut für Geochemie, Petrologic und Lagerstättenkunde, University of Frankfurt, Senckenberg-Anlage 28, D-6000 Frankfurt, FR Germany
H. Nielsen
Affiliation:
Stable Isotope Laboratory, Geochemisches Institut, University of Göttingen, Goldschmidt-Str. 1, D-3400 Göttingen, FR Germany
I. Chunnett
Affiliation:
Black Mountain Mineral Development Company (Pty) Ltd., Private Bag XO1, Aggeneys, CP 8893, Rep. of South Africa
A. Rozendaal
Affiliation:
O'okiep Copper Company Ltd., PO Box 17, Nababeep, CP 8265, Rep. of South Africa
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Abstract

Sulphur isotope ratios in sulphides and baryte from stratabound and stratiform orebodies in a metavolcanic-sedimentary sequence in Namaqualand were found, in part, to be extreme for Precambrian sulphur. Black Mountain, Aggeneys, in the west gave an average for the sulphides of δ34S = +8.9±3.7‰ (9 samples), an average for barytes of +20.6±4.3‰ (3 samples). Broken Hill, Aggeneys, in the centre gave an average for the sulphides of δ34S = +19.8±3.1‰ (19 samples). Gamsberg, in the east, gave an average for the sulphides of δ34S = +29.2±1.8‰ (24 samples), and an average for barytes of +35.4±0.2‰ (2 samples). The δ34S values increase eastward. Their range is strongly on the positive side and does not centre around zero. The Gamsberg barytes and most Gamsberg sulphides have more positive δ34S values than those reported for other Precambrian sulphides and sulphates. We interpret the above sulphur isotope range as being mainly due to the varying contributions of submarine-exhalative sulphide sulphur with δ34S close to zero and bacterially(?) reduced sulphate with strongly positive δ34S, apparently from evaporites in the east. Metamorphism of amphibolite facies grade has partly isotopically re-equilibrated the ore minerals, as indicated by galena-pyrrhotine and sulphide-baryte isotope temperatures from single specimens, but has not destroyed the primary sulphur isotope range indicating pre-existing sulphate concentrations.

Type
Research Article
Information
Mineralogical Magazine , Volume 47 , Issue 345 , December 1983 , pp. 481 - 486
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1983

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References

Barton, E. S. (1981) Geochronology. In Blignault H. J., 21–4.Google Scholar
Blignault, H. J. (compiler) (1981) Western Namaqualand Excursion, South African Geodynamics Project, GSSA, Geocongress ‘81, 50 pp., 2 maps.Google Scholar
Chadwick, J. R. (1981) World Mining, March 1981, 36–9.Google Scholar
Coetzee, C. B. (1940) Trans. R. Soc. S. Afr. 228, 199-205.CrossRefGoogle Scholar
GSSA (1975) Pre-Congress Excursion Guide Book No. 2, GSSA, 16th Geocongress.Google Scholar
Gwosdz, W., and Krebs, W. (1977) Trans. Inst. Mining Metall. 86, B73–7.Google Scholar
Koppel, V. (1980) Lead isotope studies of stratiform ore deposits of the Namaqualand, NW Cape Province, South Africa, and their implications on the age of the Bushmanland sequence. In Proc. 5 th IAGOD Symp., Ridge, J. D. (ed.), 1, 195–207.Google Scholar
Monster, J., Appel, P. W. U., Thode, H. G., Schidlowski, M., Carmichael, C. M., and Bridgwater, D. (1979) Geochim. Cosmochim. Acta 43, 405–13.CrossRefGoogle Scholar
Moore, J. M. (1980) Palaeo-environmental implications of the origin of sillimanite-rich rocks in the North-West Cape, South Africa, and their relations to sulfide deposits of the area. In Proc. 5th IAGOD Symp., (Ridge, J. D., ed.), 1, 209–15.Google Scholar
Ohmoto, H., and Lasaga, A. C. (1983) Kinetics of reactions between aqueous sulphates and sulphides in hydrothermal systems (in press).Google Scholar
Reid, D. L. (1981) Sm-Nd ages from the Namaqua and Richtersveld provinces. In Abstr., S. Afr. Geodynamics Project, 173–4, GSSA, Geocongress ‘81.Google Scholar
Rozendaal, A. (1976) The geology of the Gamsberg zinc deposit. M.Sc. thesis, Univ. of Stellenbosch.Google Scholar
Rozendaal, A. (1977) Geological structure of the Gamsberg zinc deposit, Namaqualand, South Africa. Ann. Univ. Stellenbosch, Ser. Al, 2, 1-32.Google Scholar
Rozendaal, A. (1978) In Mineralization in metamorphic terranes, (Verwoerd, W. J., ed.), GSSA Spec. Publ. 4, 235–65.Google Scholar
Rozendaal, A. (1980) The Gamsberg zinc deposit, South Africa: a banded stratiform base-metal sulphide ore deposit. In Proc. 5th IAGOD Symp. (J. D. Ridge, ed.), 1, 619-33.Google Scholar
Rozendaal, A. (1982) The petrology of the Gamsberg zinc deposit and Bushmanland iron formations with special reference to their relationships and genesis. Unpubl. Ph.D. thesis, Univ. of Stellenbosch, 349 pp.Google Scholar
Russell, M. J. (1974) Trans. Inst. Mining Metall. 83, B65–6.Google Scholar
Ryan, P. J. (1982) The geology of the Broken Hill ore deposit, Aggeneys, South Africa. In Proc. 12th CM MI Congr. (Glen, H. W., ed.), S. Afr. Inst. Min. Metall./Geol. Soc. S. Afr., 181–92.Google Scholar
Lawrence, A. L., Lipson, R. D., Moore, J. M., Paterson, A., Stedman, D. P. and van Zyl, D. (1982) Inform. Circ. 160, Econ. Geol. Res. Unit, Univ. Witwatersrand, 33 pp.Google Scholar
Stanton, R. L. (1976) Trans. Inst. Mining Metall. 85, B132–41.Google Scholar
Stumpfl, E. F. (1977) Phil. Trans. R. Soc. Lond. A286, 507–25.Google Scholar
Stumpfl, E. F. (1979) Mineral. Deposita, 14, 207–17.CrossRefGoogle Scholar
Wilson, J. D. (1981) The geology of the Broken Hill deposit, Aggeneys, North West Cape. In Abstr., S. Afr. Geodynamics Project, 231–3, GSSA, Geocongress ‘81.Google Scholar